12 resultados para 13077-059

em Chinese Academy of Sciences Institutional Repositories Grid Portal


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The piezoelastodynamic field equations are solved to determine the crack velocity at bifurcation for poled ferroelectric materials where the applied electrical field and mechanical stress can be varied. The underlying physical mechanism, however, may not correspond to that assumed in the analytical model. Bifurcation has been related to the occurrence of a pair of maximum circumferential stress oriented symmetrically about the moving crack path. The velocity at which this behavior prevails has been referred to as the limiting crack speed. Unlike the classical approach, bifurcation will be identified with finite distances ahead of a moving crack. Nucleation of microcracks can thus be modelled in a single formulation. This can be accomplished by using the energy density function where fracture initiation is identified with dominance of dilatation in relation to distortion. Poled ferroelectric materials are selected for this study because the microstructure effects for this class of materials can be readily reflected by the elastic, piezoelectic and dielectric permittivity constants at the macroscopic scale. Existing test data could also shed light on the trend of the analytical predictions. Numerical results are thus computed for PZT-4 and compared with those for PZT-6B in an effort to show whether the branching behavior would be affected by the difference in the material microstructures. A range of crack bifurcation speed upsilon(b) is found for different r/a and E/sigma ratios. Here, r and a stand for the radial distance and half crack length, respectively, while E and a for the electric field and mechanical stress. For PZT-6B with upsilon(b) in the range 100-1700 m/s, the bifurcation angles varied from +/-6degrees to +/-39degrees. This corresponds to E/sigma of -0.072 to 0.024 V m/N. At the same distance r/a = 0.1, PZT-4 gives upsilon(b) values of 1100-2100 m/s; bifurcation angles of +/-15degrees to +/-49degrees; and E/sigma of -0.056 to 0.059 V m/N. In general, the bifurcation angles +/-theta(0) are found to decrease with decreasing crack velocity as the distance r/a is increased. Relatively speaking, the speed upsilon(b) and angles +/-theta(0) for PZT-4 are much greater than those for PZT-6B. This may be attributed to the high electromechanical coupling effect of PZT-4. Using upsilon(b)(0) as a base reference, an equality relation upsilon(b)(-) < upsilon(b)(0) < upsilon(b)(+) can be established. The superscripts -, 0 and + refer, respectively, to negative, zero and positive electric field. This is reminiscent of the enhancement and retardation of crack growth behavior due to change in poling direction. Bifurcation characteristics are found to be somewhat erratic when r/a approaches the range 10(-2)-10(-1) where the kinetic energy densities would fluctuate and then rise as the distance from the moving crack is increased. This is an artifact introduced by the far away condition of non-vanishing particle velocity. A finite kinetic energy density prevails at infinity unless it is made to vanish in the boundary value problem. Future works are recommended to further clarify the physical mechanism(s) associated with bifurcation by means of analysis and experiment. Damage at the microscopic level needs to be addressed since it has been known to affect the macrocrack speeds and bifurcation characteristics. (C) 2002 Published by Elsevier Science Ltd.

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全球正在迅速工业化、城市化和现代化,当今世界一切环境污染、生态破坏问题无一不与工业化、城市化过程相联系。城市的发展对生态学提出了挑战。同样,景观生态学如何服务于城市,如何为城市的可持续发展,解决城市所面临的各种环境问题,这是广大景观生态学工作者义不容辞的责任。本文应用GIS技术,以沈阳市城市核心区(三环高速公路以内区域)为研究对象,应用景观生态学的理论与方法,探讨城市景观结构及景观与生态环境质量的关系,运用尺度分析方法来进行景观分区,探讨城市景观生态规划问题,以增加城市景观生态研究实例,补充与完善景观生态的理论与方法,为沈阳市城市景观生态建设提供理论依据。通过对其空间结构分析得出,该研究区内的景观多样性指数为2.847,优势度指数为1.059,聚积度指数为0.803。研究表明,在城市景观中存在着一明显的交错带,在该带中,景观多样性最大,。斑块数破碎化指数最大,优势度最小,均匀度最大,表明该带异质性最大,它处在郊区农业生态系统向城市中心过渡的过渡带,由于两个系统各自的能流与物流特征都可在该带内出现,所以集中了城市系统内部信息和郊区农业生态系统信息,使得该带内信息量最大,生态过程最强,这一交错带是信息流集中和汇集的焦点,是景观生态的活跃地带,对沈阳市而言,该带是一环路与二环路之间的区域。城市中人为利用开发程度从市中心向周边地区扩张,沈阳市建成区用地扩张的主要特点是条带发展带动区域扩张,局部突出促进整体发展,局部带动区域,区域带动全市,使城市用地规模不断增加,城区界限不断外延。尺度分析在景观生态学中越来越受到重视,本文应用尺度分析方法把沈阳市城市景观分为12个景观区,通过分区研究表明,沈阳市景观区布局不合理。结构决定功能,沈阳市城市环境质量状况与其景观结构有着密切的关系。不同类型的景观中,污染物含量的高低,因污染物的不同而异。TSP、SO2、NOx是工业景观中最多,绿地景观中最少,CO是道路中最多,绿地中最少。工业景观是环境污染的主要来源之一,这与工业本身的特点密切相关。沈阳市大气环境质量的空间分布状况与其景观结构密不可分。最后对城市景观生态规划的理论问题作了探讨,并提出了沈阳市城市景观生态规划的基本思路。

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分析球形水窖空间结构的应力分布情况并进行几何尺寸优化,避免建设者根据经验来确定球形水窖的厚度、构造及混凝土标号,以节省建窖材料,同时防止应力不足而发生破坏。【方法】利用基于ANSYS平台新开发的窖体有限元分析软件,对实际中窖壁厚度为4和11 cm的混凝土薄壳球形水窖进行空间结构应力分析,同时以水窖耗材量最小为目标函数,以许用应力和变形量为约束条件,对其进行几何尺寸优化。【结果】计算得出窖壁厚度为4和11 cm的水窖最大拉应力分别为1 380.00和447.31 kPa,最大压应力分别为5 153.20和1 896.70 kPa;优化出空窖不利工况下容积为20,30和40 m3的球形水窖窖壁最佳厚度,即栗钙土地区分别为0.051,0.061和0.065m,黄土地区分别为0.050,0.059和0.062 m。【结论】经软件优化计算后的球形水窖结构,既能满足强度和刚度的要求,同时也最大限度地节约了材料用量;利用新开发的窖体结构优化分析软件,能够对球形水窖进行空间应力分析与结构优化,可以作为球形水窖设计软件。

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景观结构是景观生态学研究的主要内容之一,景观结构指数多是针对农业景观和林业景观提出来的。应用GIS技术,对沈阳市城市景观结构进行了分析,结果是:景观多样性指数2.847,优势度指数1.059,聚集度指数0.803,均匀度指数58.2%,斑块密度3.7个/km2,一环内斑块密度8.825个/km2,道路密度5.52 km/km2,水系密度0.198 km/km2。结论是:目前常用的景观指数适于城市景观。沈阳市城市景观结构不合理,工业用地过多,市政设施用地和商业服务用地严重不足。在空间布局上,工业用地占据区位条件好的市中心地带,所以,用地结构必须调整。

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Nitrogen addition to soil can play a vital role in influencing the losses of soil carbon by respiration in N-deficient terrestrial ecosystems. The aim of this study was to clarify the effects of different levels of nitrogen fertilization (HN, 200 kg N ha(-1) year(-1); MN, 100 kg N ha(-1) year(-1); LN, 50 kg N ha(-1) year(-1)) on soil respiration compared with non-fertilization (CK, 0 kg N ha(-1) year(-1)), from July 2007 to September 2008, in temperate grassland in Inner Mongolia, China. Results showed that N fertilization did not change the seasonal patterns of soil respiration, which were mainly controlled by soil heat-water conditions. However, N fertilization could change the relationships between soil respiration and soil temperature, and water regimes. Soil respiration dependence on soil moisture was increased by N fertilization, and the soil temperature sensitivity was similar in the treatments of HN, LN, and CK treatments (Q (10) varied within 1.70-1.74) but was slightly reduced in MN treatment (Q (10) = 1.63). N fertilization increased soil CO2 emission in the order MN > HN > LN compared with the CK treatment. The positive effects reached a significant level for HN and MN (P < 0.05) and reached a marginally significant level for LN (P = 0.059 < 0.1) based on the cumulative soil respiration during the 2007 growing season after fertilization (July-September 2007). Furthermore, the differences between the three fertilization treatments and CK reached the very significant level of 0.01 on the basis of the data during the first entire year after fertilization (July 2007-June 2008). The annual total soil respiration was 53, 57, and 24% higher than in the CK plots (465 g m(-2) year(-1)). However, the positive effects did not reach the significant level for any treatment in the 2008 growing season after the second year fertilization (July-September 2008, P > 0.05). The pairwise differences between the three N-level treatments were not significant in either year (P > 0.05).

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Background The application of polyethylenimine (PEI) in gene delivery has been severely limited by significant cytotoxicity that results from a nondegradable methylene backbone and high cationic charge density. It is therefore necessary to develop novel biodegradable PEI derivates for low-toxic, highly efficient gene delivery.Methods A series of novel cationic copolymers with various charge density were designed and synthesized by grafting different kinds of oligoethylenimine (OEI) onto a determinate multi-armed poly(L-glutamic acid) backbone. The molecular structures of multi-armed poly(L-glutamic acid)-graft-OEI (MP-g-OEI) copolymers were characterized using nuclear magnetic resonance, viscosimetry and gel permeation chromatography. Moreover, the MP-g-OEI/DNA complexes were measured by a gel retardation assay, dynamic light scattering and atomic force microscopy to determine DNA binding ability, particle size, zeta potential, complex formation and shape, respectively. MP-g-OEI copolymers were also evaluated in Chinese hamster ovary and human embryonic kidney-293 cells for their cytotoxicity and transfection efficiency.

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A poly(o-toluidine) (POT)/2,5-dimercapto-1,3,4-thiadiazole (DMcT) composite was prepared. When POT and DMcT are mixed in a proper solvent, POT in a medium-oxidation state is reduced, and DMcT in turn is oxidized to its soluble dimer when the molar ratio of DMcT to POT is higher than 0.5. Therefore, the composite was soluble in organic solvents such as tetrahydrofuran (THF), dimethylformamide (DMF), and N-methyl-2-pyrrolidone (NMP) and exhibited very high electroactivity, two orders of magnitude higher than that of pure POT and three orders of magnitude higher than that of pure DMcT. Molecular-level contact between POT and DMcT is the reason for the improved catalytic effect of POT on DMcT, compared to that of polyaniline on DMcT. (C) 1999 The Electrochemical Society. S0013-4651(98)08-059-8. All rights reserved.

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[CoCl4(C3H12N2)], M(r) = 276.87, monoclinic, P2(1)/n, a = 10.703 (2), b = 10.653 (1), c = 10.852 (2) angstrom, beta = 118.46 (1)-degrees, V = 1087.8 angstrom 3, Z = 4, D(x) = 1.69 g cm-3, lambda(Mo K-alpha) = 0.71073 angstrom, mu = 22.60 cm-1, F(000) = 556, T = 298 K, final R = 0.059 for 1068 unique reflections [I > 3-sigma(I)]. The Co(II) ion is coordinated by four Cl atoms in a tetrahedral geometry. The paraffinic chains which bridge the tetrahedra have a nearly planar zigzag configuration.

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本研究以中国对虾为材料,以杂交育种和选择育种为目标,进行了系统的中国对虾杂交育种试验、生长性状遗传参数试验及其分子遗传连锁图谱的构建工作。结果表明以不同地理群体杂交作为基础群体,然后采用系统的选择育种方法可以获得较好的选择效果。构建的遗传连锁图谱为中国对虾分子辅助育种提供一定的基础。这些试验结果为中国对虾合理系统的育种工作提供了理论基础和数据支持。其具体结果如下: 1. 试验对中国对虾黄渤海水域乳山湾群体(WYP)和朝鲜半岛南海群体(WKN)的2个群体及其杂交后代不同月龄生长情况和存活率进行了研究,测量体长(TL)、头胸甲长(CL)、头胸甲宽(CW)、第2、3腹节高(HST)、第2、3腹节宽(WST)、体重(BW)和存活率共7个性状,计算各项指标的杂种优势率,并对各性状进行了方差分析和多重比较。其3月龄生长情况和存活率研究结果表明,存活率在乳山湾群体(WYP♀)× 朝鲜半岛南海群体(WKN♂)杂交后代出现杂种劣势外,其他指标都表现出不同程度的杂种优势(4.37%~23.96% )。除了存活率外,杂交后代生长性状均显著高于亲本,乳山湾群体(WYP♀)×朝鲜半岛南海群体(WKN♂)杂交后代高于朝鲜半岛南海群体(WKN♀)× 乳山湾群体(WYP♂)杂交后代,黄渤海水域乳山湾群体高于朝鲜半岛南海群体后代。为确定测量性状与中国对虾体重的相关程度,建立了用体长(X1),头胸甲宽(X2),第2、3腹节宽(X3),头胸甲长(X4),第2、3腹节高(X5)估计体重的多元回归方程:Y = -2.056 + 0.03X1 + 0.076X2 + 0.078X3 + 0.033X4 + 0.043X5。 2. 中国对虾黄渤海水域乳山湾群体(WYP)和朝鲜半岛南海群体(WKN)2个群体及其杂交后代在4月龄时期的6个生长指标和存活率的杂种优势范围在0.514%到14.95%之间,WYP♀×WKN♂杂交后代在这7个指标中都高于WKN♀×WYP♂杂交后代。5月龄杂交后代也表现出一定程度的杂种优势,其范围在-9.000%~19.090%之间,但头胸甲长、第2、3腹节处高和存活率3个指标出现杂种劣势。不同杂交组合各个阶段生长发育情况和存活率在杂种优势表现出一定的规律。随着月龄的增加,WKN♀×WYP♂杂交后代杂种优势率有所增加,而WYP♀×WKN♂杂交后代的却有所降低。ANOVA分析结果表明,杂交后代在存活率方面与双亲差异不显著。4月龄的分析结果发现杂交后代在WST和BW这2个指标上存在显著差异。LSD多重比较结果显示,WYP♀×WKN♂杂交后代在BW指标上与亲本存在显著差异,在WST指标方面与其他3个组合的后代差异显著。5月龄的数据分析结果发现,杂交后代除体重存在显著差异外,其他各项指标差异均不显著。LSD多重比较结果发现,WKN♀×WYP♂杂交后代体重与其亲本WKN存在显著差异。 3. 对2个野生群体——朝鲜半岛南海岸群体(WKN)和黄渤海群体(WYP)和3个养殖群体——朝鲜半岛群体的养殖一代(FKN),黄海1号(HH1)和即抗98(JK98)进行杂交试验的研究,结果表明JK98 (♀)  WKN (♂)组合在存活率方面最高,其余的依次为WYP (♀) WKN (♂),WKN (♀) WYP (♂),FKN (♀)HH1 (♂) 和 WYP (♀) FKN (♂)。而在体重方面FKN(♀)  HH1(♂)组合最高,其余的依次为WKN (♀) WYP (♂),WYP (♀) WKN (♂),WYP (♀)FKN (♂) 和 JK98 (♀)WKN (♂)。在所有生长性状方面,JK98 (♀)  WKN (♂)在5个组合中是最低的。方差检测结果表明,TL、CL、HST、LL和BW这5个指标在不同组合间存在差异,而其他指标不存在差异。多重比较结果发现JK98 (♀)WKN (♂)组合的TL与其他组合间差异极显著,HST指标与WKN (♀) WYP (♂),FKN(♀)  HH1(♂)和 WYP (♀)  WKN (♂)这3个组合差异显著,BW指标与WKN (♀) WYP (♂) 和 FKN(♀)  HH1(♂)差异显著。 4. 通过人工授精的方法建立了中国对虾21个半同胞家系,测量了中国对虾21个半同胞(46个全同胞)家系的TL、CL、CW、HST、WST、第1腹节长(FL)、第6腹节长(LL)。利用MTDFREML软件得到生长性状遗传力在0.15~0.35之间,属于中度遗传力范围。TL的遗传力为0.34±0.071,CL的为0.30±0.070,CW为0.35±0.077,WST为0.33±0.073,HST为0.33±0.073,FL的最低为0.15±0.044,LL的为0.24±0.059。各个性状间表现出高的正相关,其中CW和TL以及HST的遗传相关最大,FL和WST的遗传相关最小。 通过以上杂交育种和选择育种的研究,认为单纯的依靠杂交育种来改善中国对虾的育种工作可能具有一定的局限性。所以在实际的育种过程中,以中国对虾不同群体的杂交后代作为基础群体,并以此为基础进行系统的选择育种应该具有更大的潜力。 5. 本试验利用中国对虾F2群体和AFLP分子标记技术进行了遗传连锁图谱的构建。利用55对AFLP引物组合对F2家系的110个个体进行了研究,结果检测到532个符合作图策略的AFLP标记。利用卡方检验检测分离位点是否符合孟德尔分离定律。对于符合3:1比例的分离位点利用F2自交模型构建性别平均连锁图谱,对于符合1:1比例的分离位点利用拟测交理论分别构建中国对虾的雌性和雄性遗传连锁图谱。雌性、雄性和性别平均遗传图谱分别有28、35和44个连锁群,图谱实际长度分别为1090、1617和1772.1 cM。中国对虾遗传连锁图谱估计基因组长度为2420 cM,符合与人类基因组相比的对虾类基因组长度。中国对虾雄性遗传连锁图谱比雌性遗传连锁图谱长32.6%,这可能说明中国对虾不同性别存在不同的重组率。通过皮尔逊相关系数检测认为AFLP标记在中国对虾图谱上分布均匀。本文利用AFLP标记构建的中国对虾遗传连锁图谱为中国对虾基因组研究和遗传改良提供一定的基础,同时也应该开发微卫星等共显性标记,为遗传连锁图谱的整合提供条件。

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沉积物再悬浮作为一个比较普遍的物理现象,对浅海生态系统污染物的生物地球化学循环具有强烈的干扰作用。本研究以我国北方重要养殖海湾——桑沟湾为研究对象,从物理、化学、生物三个角度出发,研究了沉积物再悬浮的发生过程以及再悬浮介质-沉积物的源汇转换角色及其与养殖藻类的关系,构建了波流耦合模型和再悬浮颗粒物浓度预测数学模型。主要研究结果如下: 1)桑沟湾的海湾动力比约为1.54,沉积物具有发生再悬浮的潜在动力条件;推导出波流耦合切应力的计算公式。 2)悬浮颗粒物浓度(SSC)与浊度(NTU)之间符合线性方程SSC=15.908×ln(NTU)+7.0888(n=33,R2=0.7209);碎屑有机碳库是桑沟湾养殖生态系统中最大的有机碳库,占总POC库储量的81.87%。 3)沉积物再悬浮的临界切应力在0.059 N/m2左右,耦合切应力与悬浮颗粒物浓度符合方程= 238.06 SSC + 25.215(n=25,R2 = 0.7298);最大剪切深度可达8.81 cm;桑沟湾沉积物再悬浮通量的数量级在10-5~10-6 kg·m-2·s-1之间,再悬浮临界风速约为5.51 m/s,全年约有171天沉积物处于再悬浮状态;构建了沉积物再悬浮颗粒物浓度预测数学模型。 4)桑沟湾表层沉积物总氮的含量范围313.09~1094.44µg/g,有机氮是总氮的主要形态,平均占总氮的60.86%;交换态氮是无机氮的主要形式,平均占无机氮的71.40%,交换态氮中NO3--N的含量最大;桑沟湾表层沉积物的TOC/TN比值为9.38,表明沉积物中有机质具有混合来源的特征;无机磷是桑沟湾表层沉积物中磷的主要形态,平均占总磷的73.33%,钙结合磷是无机磷的主要赋存形态;表层沉积物中潜在生物有效性磷的含量占总磷的86.54%,具有很强的释磷潜力。桑沟湾重金属的潜在生态危害指数RI约为36.17,表明重金属的潜在生态危害轻微。 5)再悬浮过程中沉积物春季表现为氮磷源,释放溶解无机氮和磷酸盐;夏、秋季表现为氮汇磷源,释放磷酸盐而吸附溶解无机氮;冬季表现为氮磷汇,吸附磷酸盐和溶解无机氮。

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南岭地区是我国最重要的有色、稀有金属矿产资源产地,尤以钨、锡等金属的大规模爆发式成矿而闻名于世,已发现了一大批大型、超大型稀有和有色金属矿床。近年来的研究发现,这些矿床的形成很可能与华南地区中生代发生的大规模地壳拉张、岩石圈伸展减薄以及壳―幔相互作用的独特地质背景有关。本论文以与千里山花岗岩体密切相关的柿竹园钨锡钼铋铅锌矿田(以下简称柿竹园矿田)为研究对象,运用流体包裹体、稳定同位素和稀有气体同位素地球化学等方法,对其成矿流体的物理化学特征、来源及演化进行了研究,并在此基础上探讨了千里山花岗岩体与柿竹园矿田间的成因联系和矿田的成矿作用机制,获得以下主要研究成果: 1. 利用流体包裹体岩相学、显微测温学以及包裹体成分的激光拉曼分析技术,揭示了矿田中柿竹园钨锡钼铋矿床成矿流体的性质和演化特征。研究表明柿竹园钨锡钼铋矿床成矿流体为中高温、中高盐度H2O-NaCl-CaCl2-CO2-CH4-H2S-F体系。成矿流体的均一温度、盐度、密度和压力变化范围均较大,成矿早期夕卡岩阶段和云英岩阶段的流体具有较高的均一温度(239~477℃)和盐度(0~39.08 wt% NaCl eq.),云英岩网脉夕卡岩阶段和后期石英萤石脉阶段均一温度和盐度逐渐降低(分别为160~450℃,1.23~16.53 wt% NaCl eq.和156~340℃,1.23~4.49 wt% NaCl eq.)。夕卡岩阶段发生了流体沸腾作用。流体密度为0.37~1.12 g/cm3,主要集中在0.7~0.9 g/cm3;压力为10~820 bar,一般小于800 bar。野鸡尾锡铜矿床的成矿流体属于中高温度、中等盐度的H2O-NaCl-CaCl2-CO2-CH4-H2S-F型体系,柴山铅锌矿床属中温中等盐度H2O-NaCl-CaCl2-CO2-F体系,其均一温度和压力变化范围也较大。 2. 通过分析主要矿化类型矿石矿物及脉石矿物的C、H、O、S等稳定同位素特征,揭示了柿竹园矿田成矿流体的来源,并对C、O同位素的组成进行了CO2去气、流体混合和水―岩反应的理论模拟。研究表明矿田成矿流体主要来自千里山花岗岩浆,并有大气降水加入。水―岩反应在成矿过程中起着重要作用。 3. 对矿田不同矿化类型矿石矿物黄铁矿、黄铜矿、毒砂、方铅矿等进行了He、Ar同位素研究,其中3He/4He值为0.059~1.662 Ra(Ra为空气的3He/4He值,1 Ra=1.39×10-6),40Ar/36Ar值为289.8~1071.8,表明矿田成矿流体具有壳-幔两端员混合的特征。壳源组分为获得了大量地壳放射成因4He,但获得放射成因40Ar*较少的经过地下循环的低温饱和大气水。而幔源组分来自千里山花岗岩浆流体,表明千里山花岗岩并非传统的S型花岗岩。 4. 在总结前人研究成果的基础上,结合本次研究,建立了柿竹园矿田成矿作用模式:中生代华南岩石圈发生拉张、伸展作用,地幔物质上涌,发生壳幔相互作用,形成千里山花岗岩浆。花岗岩浆充分分异演化形成富含挥发分和成矿元素的成矿流体,与泥盆系碳酸盐岩发生反应而沉淀成矿。成矿过程有大气降水的加入,并发生了流体沸腾作用。